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wdc-climate.de:3970929 eng; USA collection ModE-RA_s14203-18501 Dr. Jörg Franke University of Bern not filled pointOfContact 2023-03-22T14:59:14 ISO 19115 ISO 19115-2:2009 ModE-RA - A global monthly paleo-reanalysis of the modern era (1421 to 2008): Set 1420-3_1850-1 2023-04-19 publication 1 ModE-RA_s14203-18501 doi:10.26050/WDCC/ModE-RA_s14203-18501 Dr. Jörg Franke University of Bern not filled Email: franke@giub.unibe.ch principalInvestigator Dr. Veronika Valler University of Bern not filled Email: veronika.valler@giub.unibe.ch author Dr. Jörg Franke University of Bern not filled Email: franke@giub.unibe.ch author Yuri Brugnara University of Bern not filled Email: yuri.brugnara@gmail.com author Angela-Maria Burgdorf University of Bern not filled Email: angela-maria.burgdorf@giub.unibe.ch author Elin Lundstad University of Bern not filled Email: elin.lundstad@giub.unibe.ch author Dr. Ralf Hand University of Bern not filled Email: ralf.hand@giub.unibe.ch author Dr. Eric Samakinwa University of Bern not filled Email: eric.samakinwa@giub.unibe.ch author Laura Lipfert University of Bern not filled Email: laura.hoevel@giub.unibe.ch author Andrew Ronald Friedman University of Bern not filled Email: andrew.friedmann@giub.unibe.ch author Prof. Dr. Stefan Brönnimann University of Bern not filled Email: stefan.broennimann@giub.unibe.ch author WDC Climate at DKRZ publisher not filled Dr. Jörg Franke University of Bern not filled pointOfContact NetCDF CSV Paleo-Reanalyse climate reconstruction early instrumental measurements historic documents historical large ensemble modern era climate palaeo reanalysis proxy data re-analysis CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA -180.0 180.0 -90.0 90.0 proleptic_gregorian 1421-01-01 2008-12-31 info:eu-repo/grantAgreement/EC/H2020/787574/BE//PA Palaeoreanalysis To Understand Decadal Climate Variability (PALAEO-RA) geopotential_height-at500hPa Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name-vertical_coordinate]; unit: m air_temperature-at2m Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name-vertical_coordinate]; unit: K not filled not filled; unit: not filled air_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa northward_wind-at850hPa "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name-vertical_coordinate]; unit: m s-1 eastward_wind-at850hPa "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name-vertical_coordinate]; unit: m s-1 geopotential_height-at500hPa Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name-vertical_coordinate]; unit: m northward_wind-at850hPa "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name-vertical_coordinate]; unit: m s-1 precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 air_temperature-at2m Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name-vertical_coordinate]; unit: K air_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa lagrangian_tendency_of_air_pressure-at500hPa "tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name-vertical_coordinate]; unit: Pa s-1 lagrangian_tendency_of_air_pressure-at500hPa "tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name-vertical_coordinate]; unit: Pa s-1 eastward_wind-at850hPa "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name-vertical_coordinate]; unit: m s-1 NetCDF CSV 143121 https://www.wdc-climate.de/ui/entry?acronym=ModE-RA_s14203-18501 information collection